Articles | Volume 12, issue 10
https://doi.org/10.5194/gmd-12-4443-2019
https://doi.org/10.5194/gmd-12-4443-2019
Development and technical paper
 | 
24 Oct 2019
Development and technical paper |  | 24 Oct 2019

Improving permafrost physics in the coupled Canadian Land Surface Scheme (v.3.6.2) and Canadian Terrestrial Ecosystem Model (v.2.1) (CLASS-CTEM)

Joe R. Melton, Diana L. Verseghy, Reinel Sospedra-Alfonso, and Stephan Gruber

Viewed

Total article views: 3,164 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,126 952 86 3,164 213 91 85
  • HTML: 2,126
  • PDF: 952
  • XML: 86
  • Total: 3,164
  • Supplement: 213
  • BibTeX: 91
  • EndNote: 85
Views and downloads (calculated since 12 Apr 2019)
Cumulative views and downloads (calculated since 12 Apr 2019)

Viewed (geographical distribution)

Total article views: 3,164 (including HTML, PDF, and XML) Thereof 2,788 with geography defined and 376 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Jan 2025
Download
Short summary
Soils in cold regions store large amounts of carbon that could be released to the atmosphere if the soils thaw. To best simulate these soils, we explored different configurations and parameterizations of the CLASS-CTEM model and compared to observations. The revised model with a deeper soil column, new soil depth dataset, and inclusion of moss simulated greatly improved annual thaw depths and ground temperatures. We estimate subgrid-scale features limit further improvements against observations.